Poznámky k recentní dynamice suťových svahů v Českém středohoří

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F44555601%3A13440%2F07%3A00004208" target="_blank" >RIV/44555601:13440/07:00004208 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Comments on the recent dynamics of scree slopes

Popis výsledku v původním jazyce

Scree slopes have been actually long recognized as significant landforms in a landscape, which represent the indicators of palaeogeographical development of a territory on one hand, and the specific recent environment on the other. The origin and primarydevelopment of these landforms was traditionally related to the Last Glacial, resp. Dansgaard-Oeschger cycles, however, the progress in geomorphologic research of scree slopes during last few decades indicated, that these might have evolved continuouslyduring the Holocene period. Our research, which was carried out in the Czech Middle Mountains in north-western Czechia was focused on evidences of the recent dynamics of scree slopes and their environmental change. Dendrogeomorphologic and dendrochronologic analyses showed the evidences of rock-fall, i.e. continuous formation of scree, at least 15 years back. Moreover, sedimentologic analyses of clast size, distribution, and shallow profiles indicated the probable climatic multifactor i

Název v anglickém jazyce

Comments on the recent dynamics of scree slopes

Popis výsledku anglicky

Scree slopes have been actually long recognized as significant landforms in a landscape, which represent the indicators of palaeogeographical development of a territory on one hand, and the specific recent environment on the other. The origin and primarydevelopment of these landforms was traditionally related to the Last Glacial, resp. Dansgaard-Oeschger cycles, however, the progress in geomorphologic research of scree slopes during last few decades indicated, that these might have evolved continuouslyduring the Holocene period. Our research, which was carried out in the Czech Middle Mountains in north-western Czechia was focused on evidences of the recent dynamics of scree slopes and their environmental change. Dendrogeomorphologic and dendrochronologic analyses showed the evidences of rock-fall, i.e. continuous formation of scree, at least 15 years back. Moreover, sedimentologic analyses of clast size, distribution, and shallow profiles indicated the probable climatic multifactor i

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

<a href="/cs/project/1J008%2F04-DP1" target="_blank" >1J008/04-DP1: Metodika hodnocení sociálních a ekologických souvislostí ekonomické transformace: teorie a aplikace</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2007

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

GEOMORPHOLOGIA SLOVACA

ISSN

1335-9541

e-ISSN

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Svazek periodika

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Číslo periodika v rámci svazku

VII/1

Stát vydavatele periodika

SK - Slovenská republika

Počet stran výsledku

7

Strana od-do

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Kód UT WoS článku

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EID výsledku v databázi Scopus

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